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Record #131400:
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MARC recordThe lower Jyllandselv succession: evidence for three Weichselian glacier advances over coastal Jameson Land, East Greenland / Astrid Lyså, Jon Y. Landvik.
| Title: | The lower Jyllandselv succession: evidence for three Weichselian glacier advances over coastal Jameson Land, East Greenland / Astrid Lyså, Jon Y. Landvik. |
| Author(s): | Lyså, Astrid. Landvik, Jon Y. |
| Date: | 1994. |
| In: | Boreas. (1994.), Vol. 23(4) (1994) |
| Abstract: | Sediments exposed at river sections in coastal Jameson Land show Saalian to Holocene glacial history. 11 sedimentary units have been distinguished, most superimposed at one large section. Three out of four subglacial till beds are Weichselian. Tills are separated by marine, fluvial or deltaic sediments and seem to represent sea-level changes in ice-free periods.Dating is supported by fossils and luminescence. Some sedimentation was controlled by glacio- isostatic subsidence caused by net growth of Greenland Ice Sheet. |
| Notes: | Boreas. Vol. 23(4) :432-446 (1994). |
| Keywords: | 551.1/.4 -- Geology. 551.3.051 -- Sedimentation and stratification. 551.324.6 -- Land ice, fluctuation. 551.332.21 -- Till or boulder clay. Tillite. Glacial diamictites. 551.336 -- Ice ages. 551.7 -- Stratigraphy. 551.79 -- Quaternary. B -- Geology and soil sciences. (*3) -- Arctic regions. (*38) -- Greenland. (*381) -- East Greenland. (*381.4) -- Kong Christian den Xs Land. |
| SPRI record no.: | 131400 |
LDR 01720naa#a2200000#a#4500 001 SPRI-131400 005 20240419062107.0 007 ta 008 240419s1994####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-131400 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLyså, Astrid. 245 14 ‡aThe lower Jyllandselv succession :‡bevidence for three Weichselian glacier advances over coastal Jameson Land, East Greenland /‡cAstrid Lyså, Jon Y. Landvik. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1994. 300 ## ‡ap. 432-446 :‡bill., diags., tables, maps. 500 ## ‡aBoreas. Vol. 23(4) :432-446 (1994). 520 3# ‡aSediments exposed at river sections in coastal Jameson Land show Saalian to Holocene glacial history. 11 sedimentary units have been distinguished, most superimposed at one large section. Three out of four subglacial till beds are Weichselian. Tills are separated by marine, fluvial or deltaic sediments and seem to represent sea-level changes in ice-free periods.Dating is supported by fossils and luminescence. Some sedimentation was controlled by glacio- isostatic subsidence caused by net growth of Greenland Ice Sheet. 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc 650 07 ‡a551.324.6 -- Land ice, fluctuation.‡2udc 650 07 ‡a551.332.21 -- Till or boulder clay. Tillite. Glacial diamictites.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.7 -- Stratigraphy.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*38) -- Greenland.‡2udc 651 #7 ‡a(*381) -- East Greenland.‡2udc 651 #7 ‡a(*381.4) -- Kong Christian den Xs Land.‡2udc 700 1# ‡aLandvik, Jon Y. 773 0# ‡7nnas ‡tBoreas. ‡gVol. 23(4) (1994) ‡wSPRI-56035 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419